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The lagoa Pitanguinha has an area of approximately 0.55 km², of which 1.5 km are in length, it is located between the latitudes of 22° 55’42’’and 22° 56’00’’ S and longitudes of 42°20’45’’ and 42°20’30’’ W, at the restinga de Massambaba, near the district of Araruama. The microbial mats are laminate organosedimentarystructures and have been called “algal mat”, “cyanobacteria mat” and “potential stromatolite”, because there is the predominance of cyanobacteria species that are responsible for the formation of the laminate sediment structure. These mats are the oldest known ecosystem. The aim of this study is to determine the geomicrobiologyand sedimentary composition of film microbial mats at lagoa Pitanguinha. The film mat appeared to be placed at the intertidal region and has the form of a flat laminae, with a porous and coherent aspect, being composed of lithified sediment compound with crystalclear incrustation. In its inner side the presence shell fragment of bivalve, microgastropod, ostracod and quartz grains of sand size. The main species of cyanobacteria present in the film microbial mat is Entophysalis granulosa Kützing 1843. On the superficial layers of the film microbial mats, sediment grains are much more united due to the presence of filament cyanobacteria that traps and unitesthe sediment. The rest of the space is filled by spherical cyanobacteria. On deeper layers of the film microbialmats, sediment grains are much more scattered, due to the presence of few filament cyanobacteria and many spherical ones. |
